Difference between revisions of "Ozone"

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It is unstable at standard temperatures and pressures, and a powerful [[oxidizer]].  At the earth's surface it occurs naturally as a result of electrical discharges, most prominently, [[lightning]].  It is also created by [[man-made]] sparks, such as in an electrical motor.   
 
It is unstable at standard temperatures and pressures, and a powerful [[oxidizer]].  At the earth's surface it occurs naturally as a result of electrical discharges, most prominently, [[lightning]].  It is also created by [[man-made]] sparks, such as in an electrical motor.   
  
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In the upper atmosphere it serves a very important function, by acting to filter out most of the sun's ultraviolet radiation.   
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In the stratosphere it serves a very important function, by acting to filter out most of the sun's ultraviolet radiation.   
  
 
Some activists claimed that this ozone layer has been threatened in recent decades by the release of [[chlorofluorocarbons]], on the theory that these act as [[catalyst]]s to break down the O<sub>3</sub> molecules.
 
Some activists claimed that this ozone layer has been threatened in recent decades by the release of [[chlorofluorocarbons]], on the theory that these act as [[catalyst]]s to break down the O<sub>3</sub> molecules.

Revision as of 21:52, May 8, 2007

Ozone is a chemical compound consisting of three oxygen atoms. It is represented by the symbol O3.

It is unstable at standard temperatures and pressures, and a powerful oxidizer. At the earth's surface it occurs naturally as a result of electrical discharges, most prominently, lightning. It is also created by man-made sparks, such as in an electrical motor.

In the stratosphere it serves a very important function, by acting to filter out most of the sun's ultraviolet radiation.

Some activists claimed that this ozone layer has been threatened in recent decades by the release of chlorofluorocarbons, on the theory that these act as catalysts to break down the O3 molecules.